The Atmosphere and the Weather

The Atmosphere

An atmosphere is a layer of gases that surounds a planet. Earth's atmosphere is relatively thin in vertical extent compared to the size of the solid part of the planet (see Figure). In that figure, the "habitable atmosphere" refers to the portion of the atmosphere where humans can survive without breathing assistence, which extends up to only about 6 kilometers (or 4 miles) above sea level. Thus, we must remain near sea level in a thin vertical layer (consider how short 6 kilometers seems when moving along a horizontal path). People often use the term "thin air" to describe the air at high alitudes, where "thin" refers to the density of air (the number of gas molecules that is contained in a given volume, like the volume of your lungs for example). It gets more difficult to breath as the air becomes "thinnner" or less dense. In the atmosphere, the gas density is highest at the surface and gets lower and lower as one moves away from the surface until at some point (on the order of a few hundred kilometers above sea level), it becomes difficult to determine whether you are still in the Earth's atmosphere or in outer space.

The atmosphere is retained by Earth's gravity. The mixture of gases that is found on Earth today is commonly called air. Beside gases, the atmosphere also contains very minute quantities of microscopically small suspended particles of solid and liquid (called aerosols), which includes things like dust, pollen, and cloud droplets. Most aerosols are much too small to see individually. However, when concentrations of aerosols are high, such as the microscopic liquid droplets that make up clouds, they can be seen. Gases are composed of individual molecules that are not chemically bonded together. The gas molecules and suspended aerosols are individually very tiny and have very little mass. Thus, they have very little weight on Earth compared with the solid and liquid substances that compose the Earth's ground surface. In essence, the larger and heavier solids and liquids sink to the bottom, and the gases (the atmosphere) float to the top and becomes the outer layer surrounding the Earth. Not all planets have atmospheres of gas surrounding them; yet many other planets have much more massive atmospheres than the Earth. Living on the surface of the Earth (at the bottom of the atmospere), we have become so adapted to our particular atmosphere that we cannot survive more than a few minutes without it. Just as fish need to be surrounded in an environment of water to survive, we must be surrounded in an environment of air. And anywhere we go, e.g., under water, outer space, etc., we must have air with us for long-term survival.

Meteorology is the study of the atmosphere and the processes (such as cloud formation, lightning, and the movement of the wind) that cause what we refer to as the "weather". Most of the world's weather systems and their related features, including clouds and rain, develop in the lowest layer of the atmosphere, called the troposphere. Such weather systems, or patterns of air movement, develop as a result of the flow of heat from warmer regions of the Earth near the equator to colder regions nearer the poles. The air, and the heat it carries however, does not flow in a straight line, because of the Earth's rotation. As a consequence, the air flow is deflected, forming the swirling patterns of air circulation we observe on Earth.

Despite its relative thinness, our existance is completely dependent upon the atmosphere. Essential functions of the atmosphere include:

Allows breathing, we cannot live without sufficient oxygen
Acts as a shield, protecting the surface from harmful ultraviolet (uv) radiation and other high energy particles from the Sun and space, and even meteors on a collision course with the Earth. The uv protection is provided by the gas ozone in the stratosphere.
The atmosphere transports heat and moisture creating more uniform conditions around the globe than if there were no atmosphere. Without the atmosphere, very much larger extremes in temperature would exist between the Equatorial and Polar regions than are observed. Without the atmosphere, much larger extremes in temperature would occur between day and night. The atmosphere transports water (in the form of water vapor) from oceans to land. This is essential for life on land to exist.
The atmosphere keeps the average surface temperature of the Earth much warmer than if there were no atmosphere through the Greenhouse effect. With no atmosphere (and assuming that the amount of radiation energy that the Earth absorbs from the Sun does not change), the average surface temperature of the Earth would be about 0 degrees Fahrenheit. The presence of the atmosphere keeps the average surface temperature at 59 degrees Fahrenheit.

The atmosphere also influences our existance in several non-life essential ways:

Propagation of sound. Sound does not travel through empty space (e.g., outer space)
Provides visual sights such as blue skies, clouds, rainbows, and colorful sunsets
Sense of smell is also influenced by the atmosphere